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dc.contributor.authorChelidze, T.en_US
dc.contributor.authorShengelia, Ia.en_US
dc.contributor.authorZhukova, N.en_US
dc.contributor.authorMatcharashvili, T.en_US
dc.contributor.authorMelikadze, G.en_US
dc.contributor.authorKobzev, G.en_US
dc.contributor.authorჭელიძე, თ.ka_Ge
dc.contributor.authorშენგელია, ი.ka_Ge
dc.contributor.authorჟუკოვა, ნ.ka_Ge
dc.contributor.authorმაჭარაშვილი, თ.ka_Ge
dc.contributor.authorმელიქაძე, გ.ka_Ge
dc.contributor.authorკობზევი, გ.ka_Ge
dc.date.accessioned2015-01-14T09:04:52Z-
dc.date.available2015-01-14T09:04:52Z-
dc.date.issued2014-
dc.identifier.citationBULLETIN OF THE GEORGIAN NATIONAL ACADEMY OF SCIENCES, vol. 8, no. 2, 20 14, pp. 75-79en_US
dc.identifier.urihttp://hdl.handle.net/123456789/4816-
dc.description.abstractThe dynamic triggering due to the great Tohoku M 9 earthquake Japan (2011) was observed in local seismicity all around the globe. We presume that Tohoku EQ could also trigger local seismic events in Georgia (Caucasus), which is separated from Japan by 7800 km. It was discovered during integrated analysis of seismic and water level records in wells that besides S, L and R waves, multiple surface Rayleigh waves also induce water level oscillationsen_US
dc.language.isoenen_US
dc.subjectგეოფიზიკაka_Ge
dc.subjectშრომებიka_Ge
dc.subjectსტატიაka_ge
dc.subjectTohoku earthquakeen_US
dc.subjectwater levelen_US
dc.subjectmultiple surface Rayleigh wavesen_US
dc.titleCoupling of Multiple Rayleigh Waves and Water Level Signals during 2011 Great Tohoku Earthquake Observed in Georgia, Caucasusen_US
dc.titleსაქართველოში დაფიქსირებული მრავალჯერადი რელეის ტალღების და წყლის დონის ანომალიების კავშირი 2011 წლის დიდი ტოჰოკუს მიწისძვრის დროსka_Ge
dc.typeArticleen_US
dc.typeსტატიაka_Ge
dc.date.published2014 წ.ka_Ge
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